The Geologic Time Scale Flashcards

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1
Q

Refers to the divisions of earth’s history based on life forms

A

Geologic Time Scale

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2
Q

are the largest intervals of geologic time with duration of hundreds of millions of years. The geologic time scale is divided into 4 major units

A

Eon

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3
Q

The geologic time scale is divided into 4 major units

A

Hadean Eon
Archean Eon
Proterozoic Eon
Phanerozoic Eon

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4
Q

there were fewer life forms. These life forms are more difficult to identify and the rocks have been disturbed often. An informal name given to the first three eons of the geologic time scale

A

precambrian

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5
Q

began 4.5 to 4 billion years ago. Known as the rock less eon. Except for the meteorites, no existing rocks on Earth today are from the Hadean eon. During this time, Earth was molten, and it would only solidify as it cooled.

A

hadean eon

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6
Q

began 1.5 billion years ago. during the Archean eon that single-celled organisms, such as blue-green algae, archeans, and bacteria, first appeared. It is the beginning of free oxygen in the atmosphere.

A

archean eon

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7
Q

the first era of the Archean Eon of the geologic record. Earth’s surface was dominated by volcanic activity during this era. The atmosphere consisted mainly of carbon dioxide and water vapor.

A

eroarchean era

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8
Q

The earliest confirmed evidence of life comes from this era, and Vaalbara, one of Earth’s earliest supercontinents, may have formed during this era.

A

paleoarchean era

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9
Q

the beginning of the Pongola glaciation on earth, which occurred in what is now South Africa. This was the first climate disaster on earth, as ice sheets covered areas of Swaziland and South Africa.

A

mesoarchean era

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10
Q

represents a key period in Earth’s evolution, as it recorded a transition in tectonic style, from an Early-Archean Earth dominated by episodic-overturn/stagnant-lid regime to a Proterozoic Earth in which modern- style Plate Tectonics became progressively established.

A

neoarchean era

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11
Q

began 2.5 billion years ago and ended 542 million years ago. the first continents appeared. This was also the time when continents merged into a single landmass called Rodinia. The Proterozoic eon is marked by the appearance of multicellular animals like sponges and the mass extinction of these organisms.

A

proterozoic eon

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12
Q

had given rise to crown eukaryotes, which are the ancestral organisms from which all modern eukaryotic lineages have evolved. This era is also marked by the earliest global-scale continent-continent belt collisions known.

A

paleoproterozoic era

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13
Q

are the breakup of the Columbia supercontinent, the formation of the Rodinia supercontinent, and the evolution of sexual reproduction. This era is marked by the further development of continental plates and plate tectonics.

A

mesoproterozoic era

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14
Q

is characterized by the most important climatic, tectonic and paleo - evolutionary changes in the Earth’s geological record

A

neoproterozoic era

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15
Q

The first life forms with parts, such as shells, scales, and bones and teeth, appeared during the Phanerozoic eon. The fossils of these life forms are great tools in the study of the history of the Phanerozoic eon.

A

phanerozoic eon

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16
Q

means “ancient life”. The supercontinent Pangaea was formed during the this era.

A

paleozoic era

17
Q

represents the major increase in number of invertebrates.

A

cambrian to ordovician period

18
Q

represents the evolution of fishes.

A

silurian to devonian period

19
Q

represents the evolution of amphibians.

A

carboniferous to permian

20
Q

means “middle life”. It’s a popular time division because it was when dinosaurs dominated and lived on dry land.

A

mesozoic era

21
Q

came after a recent extinction that left only a few animals. One of these animals, the Archosaur, became the prototype for the dinosaurs in the Jurassic and Cretaceous period. Today, the only known descendants of Archosaurs are birds and crocodile-like animals.

A

triassic period

22
Q

was the Golden Age of dinosaurs. Animals from the Triassic grew, spread and diversified in the Jurassic Period, making some of the most famous dinosaurs we know now today, like the T-rex. Some dinosaurs began to develop feathers, bone structures that resembled modern-day birds. This was a period when reptiles ruled all areas: land, water and air.

A

jurassic period

23
Q

marks the final period of the Mesozoic era, when all living beings reached big and great sizes, but also faced harsh competition.

A

cretaceous period

24
Q

recent life’. this era comes directly after the Mesozoic era. This era is well-known for introducing flowering plants, birds, insects and mammals, including humans.

A

Cenozoic era

25
Q

abruptly when a meteorite slammed into the earth, leading to a mass extinction that wiped out about 75% of all species on Earth. This left only a few surviving mammals and reptiles that grew to be the animals we know now in modern day.

A

tertiary period

26
Q

 “old recent”
 was the complete absence of dinosaurs and other reptilian groups
 rapid proliferation and evolution of mammals
 warm and humid climate
 continents moved closer to their current positions

A

paleocene epoch

27
Q

 ”dawn of the recent”
 marks the first appearance of fossil
 global climate is warm and rainy
 noted for the expansion of mammalian stocks

A

eocene epoch

28
Q

 ”few recent forms”
 a global expansion of grassland and forest region
 sudden decrease in earth’s temperature
 noted for the expansion of mammalian stocks

A

oligeocene epoch

29
Q

 ”less recent”
 warmer global climate than the previous epochs
 many fauna and flora died and others adapted to the drying world

A

miocene epoch

30
Q

 ”continuation of the recent”
 global climatic cooling
 growth of mountains
 animals flourished, other species died out

A

pliocene epoch

31
Q

marks the time when humans started growing and thriving until present.

A

quaternary period

32
Q

 the “Great Ice Age”
 the last time great diversity mammals lived like the mammoth

A

pleistocene epoch

33
Q

 the ”Age of Man”
 All recorded human history occurred in this epoch

A

halocene epoch